Areas of updraft air motion from WRF model simulations.

Presented dataset is a part of numerical modelling study focusing on the analysis of sea ice floes size distribution (FSD) influence on the horizontal and vertical structure of convection in the atmosphere. The total area and spatial arrangement of the updrafts indicates that the FSD affects the tot...

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Main Authors: Marta Wenta, Zakład Oceanografii Fizycznej, Instytut Oceanografii, Uniwersytet Gdański
Format: Dataset
Language:English
Published: Gdańsk University of Technology 2020
Subjects:
Online Access:https://dx.doi.org/10.34808/fwt2-bs21
https://mostwiedzy.pl/en/open-research-data/areas-of-updraft-air-motion-from-wrf-model-simulations,102042114114661-0
id ftdatacite:10.34808/fwt2-bs21
record_format openpolar
spelling ftdatacite:10.34808/fwt2-bs21 2023-05-15T18:17:31+02:00 Areas of updraft air motion from WRF model simulations. Marta Wenta Zakład Oceanografii Fizycznej, Instytut Oceanografii, Uniwersytet Gdański 2020 https://dx.doi.org/10.34808/fwt2-bs21 https://mostwiedzy.pl/en/open-research-data/areas-of-updraft-air-motion-from-wrf-model-simulations,102042114114661-0 en eng Gdańsk University of Technology numerical modeling atmosphere convection ocea-sea ice-atmosphere interactions floe size distribution numerical modelling convection in the atmosphere dataset Dataset 2020 ftdatacite https://doi.org/10.34808/fwt2-bs21 2021-11-05T12:55:41Z Presented dataset is a part of numerical modelling study focusing on the analysis of sea ice floes size distribution (FSD) influence on the horizontal and vertical structure of convection in the atmosphere. The total area and spatial arrangement of the updrafts indicates that the FSD affects the total moisture content and the values of area averaged turbulent fluxes in the model domain. In fact, while convective updrafts occur in every one of model simulations, their intensity differs with varying FSD due to the changing extent and strength of breeze-like circulation. When the floes are tightly packed in the model domain (simulations with 1000 and 5000 floes) the updrafts are numerous but weaker due to weaker breeze like circulation. In the simulations with smaller floes numbers (Nf =50 and Nf=100) the opposite situation takes place and the updrafts, while covering smaller area, are stronger and thus are the values of total moisture and area averaged heat content for the model domain, as described in Wenta and Herman (2019). Presented dataset consists of: Description of WRF model configuration and the model output post processing (Techinical_details.docx). Images of the areas of updraft air motion generated for the following simulations: Initialized with wind profile of vertically averaged wind speed of 1.06 m/s (Profile 1), sea ice concentrations (c) of 50%, 70%, 90% and five different FSDs (labelled by the number of the floes present in the model domain) of: Nf=50, Nf=100, Nf=500, Nf=1000, Nf=5000. Initialized with wind profile of vertically averaged wind speed of 2.01 m/s (Profile 2), sea ice concentration of of 50%,70%, 90% and five different FSDs (labelled by the number of the floes present in the model domain) of: Nf=50, Nf=100, Nf=500, Nf=1000, Nf=5000. Summary of total updrafts coverage for every simulation in a Microsoft Excel format. Dataset Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic numerical modeling
atmosphere
convection
ocea-sea ice-atmosphere interactions
floe size distribution
numerical modelling
convection in the atmosphere
spellingShingle numerical modeling
atmosphere
convection
ocea-sea ice-atmosphere interactions
floe size distribution
numerical modelling
convection in the atmosphere
Marta Wenta
Zakład Oceanografii Fizycznej, Instytut Oceanografii, Uniwersytet Gdański
Areas of updraft air motion from WRF model simulations.
topic_facet numerical modeling
atmosphere
convection
ocea-sea ice-atmosphere interactions
floe size distribution
numerical modelling
convection in the atmosphere
description Presented dataset is a part of numerical modelling study focusing on the analysis of sea ice floes size distribution (FSD) influence on the horizontal and vertical structure of convection in the atmosphere. The total area and spatial arrangement of the updrafts indicates that the FSD affects the total moisture content and the values of area averaged turbulent fluxes in the model domain. In fact, while convective updrafts occur in every one of model simulations, their intensity differs with varying FSD due to the changing extent and strength of breeze-like circulation. When the floes are tightly packed in the model domain (simulations with 1000 and 5000 floes) the updrafts are numerous but weaker due to weaker breeze like circulation. In the simulations with smaller floes numbers (Nf =50 and Nf=100) the opposite situation takes place and the updrafts, while covering smaller area, are stronger and thus are the values of total moisture and area averaged heat content for the model domain, as described in Wenta and Herman (2019). Presented dataset consists of: Description of WRF model configuration and the model output post processing (Techinical_details.docx). Images of the areas of updraft air motion generated for the following simulations: Initialized with wind profile of vertically averaged wind speed of 1.06 m/s (Profile 1), sea ice concentrations (c) of 50%, 70%, 90% and five different FSDs (labelled by the number of the floes present in the model domain) of: Nf=50, Nf=100, Nf=500, Nf=1000, Nf=5000. Initialized with wind profile of vertically averaged wind speed of 2.01 m/s (Profile 2), sea ice concentration of of 50%,70%, 90% and five different FSDs (labelled by the number of the floes present in the model domain) of: Nf=50, Nf=100, Nf=500, Nf=1000, Nf=5000. Summary of total updrafts coverage for every simulation in a Microsoft Excel format.
format Dataset
author Marta Wenta
Zakład Oceanografii Fizycznej, Instytut Oceanografii, Uniwersytet Gdański
author_facet Marta Wenta
Zakład Oceanografii Fizycznej, Instytut Oceanografii, Uniwersytet Gdański
author_sort Marta Wenta
title Areas of updraft air motion from WRF model simulations.
title_short Areas of updraft air motion from WRF model simulations.
title_full Areas of updraft air motion from WRF model simulations.
title_fullStr Areas of updraft air motion from WRF model simulations.
title_full_unstemmed Areas of updraft air motion from WRF model simulations.
title_sort areas of updraft air motion from wrf model simulations.
publisher Gdańsk University of Technology
publishDate 2020
url https://dx.doi.org/10.34808/fwt2-bs21
https://mostwiedzy.pl/en/open-research-data/areas-of-updraft-air-motion-from-wrf-model-simulations,102042114114661-0
genre Sea ice
genre_facet Sea ice
op_doi https://doi.org/10.34808/fwt2-bs21
_version_ 1766191780648189952